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Is Ziarat a Potential Site for Conventional or Unconventional Energy Resources?

机译:Ziarat是常规能源还是非常规能源的潜在场所?

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摘要

A structural interpretation of the Ziarat block in the Balochistan region (a part of the Suleiman Fold and Thrust Belt) has been carried out using seismic and seismological data.Seismic data consists of nine 2.5D pre-stack migrated seismic lines,whereas the seismological data covers the Fault Plane Solution and source parameters.Structural interpretation describes two broad fault sets of fore and back thrusts in the study area that have resulted in the development of pop-up structures,accountable for the structural traps and seismicity pattern in terms of seismic hazard.Seismic interpretation includes time and depth contour maps of the Dungan Formation and Ranikot group,while seismological interpretation includes Fault Plane Solution,that is correlated with a geological and structural map of the area for the interpretation of the nature of the subsurface faults.Principal stresses are also estimated for the Ranikot group and Dungan Formation.In order to calculate anisotropic elastic properties,the parameters of the rock strength of the formations are first determined from seismic data,along with the dominant stresses (vertical,minimum horizontal,and maximum horizontal).The differential ratio of the maximum and minimum horizontal stresses is obtained to indicate optimal zones for hydraulic fracturing,and to assess the potential for geothermal energy reservoir prospect generation.The stress maps indicate high values towards the deeper part of the horizon,and low towards the shallower part,attributed to the lithological and structural variation in the area.Outcomes of structural interpretation indicate a good correlation of structure and tectonics from both seismological and seismic methods.
机译:利用地震和地震数据对Bal路支斯坦地区(苏莱曼褶皱和冲断带的一部分)的Ziarat块进行了结构解释。地震数据由9条2.5D叠前偏移地震线组成,而地震数据结构解释说明了研究区域内前后推力的两大断层组,这些断层组导致了弹起结构的发展,就地震危险而言是结构性圈闭和地震活动模式的原因。地震解释包括Dungan组和Ranikot组的时间和深度等值线图,而地震解释包括断层平面解,与平面地质图相关联以解释地下断层的性质。​​主应力还估算了拉尼科特群和邓干组。为了计算各向异性弹性性能,首先从地震数据中确定地层岩石强度的参数,以及主要应力(垂直应力,最小水平应力和最大水平应力)。获得最大和最小水平应力的微分比以指示最佳区域应力图表明,地层较深的部分值较高,而地层较浅的部分值较低,这归因于该地区的岩性和结构变化。从地震学和地震学方法来看,构造解释表明构造和构造具有良好的相关性。

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  • 来源
    《地质学报(英文版)》 |2018年第4期|1544-1557|共14页
  • 作者单位

    National Centre of Excellence in Geology, University of Peshawar, Peshawar, 25130, Pakistan;

    Comsats Institute of Information and Technology, Abbottabad, Pakistan;

    Comsats Institute of Information and Technology, Islamabad, Pakistan;

    National Centre of Excellence in Geology, University of Peshawar, Peshawar, 25130, Pakistan;

    National Centre of Excellence in Geology, University of Peshawar, Peshawar, 25130, Pakistan;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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